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Retention trees slow post-harvest fine-root decomposition in a coastal temperate rainforest

机译:保留树缓慢收获后沿海温带雨林中的细根分解

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Fine roots are a dominant, but often overlooked source of carbon (C) in forest soils, and decomposition of this material may have important consequences for C storage and turnover in forest ecosystems. Forest harvesting modifies soil physicochemical properties and microbial communities, which may lead to faster decomposition rates, but the effect of harvesting on fine-root decomposition is rarely investigated. Variable-retention harvesting, where some trees are left on site after harvest, often results in lower soil moisture and temperature, and increased ectomycorrhizal diversity relative to clearcut harvesting. As such, this harvesting practice may influence fine-root decomposition rates. In Douglas-fir forests in coastal British Columbia, we measured fine-root (& 2 mm diameter) decomposition rates in variable-retention (aggregate and dispersed arrangements), clearcut, and uncut treatments, and determined if any effects persisted as stands aged. Within the variable-retention treatments, we also examined if fine-root decomposition rates varied with distance from retention trees or retention patches. Further, we determined which soil physicochemical variables best explained variation in fine-root carbon loss after two years of decomposition. Increased tree coverage slowed fine root decomposition; fine roots decomposed as slowly under variable-retention treatments as in uncut stands, and 15-19% more carbon was retained in these treatments relative to the clearcut treatment. Fine roots also decomposed faster with increasing distance from retention patches or retention trees as decomposition was twofold slower in the aggregate centre relative to open areas, with similar patterns observed in the dispersed retention treatment. However, fine roots decomposed at similar rates in forests and stands with more advanced regeneration, suggesting the effects of harvesting on decomposition rates was not persistent. Across all sampling locations, 37% of the variation in fine-root carbon loss was explained by fine-root biomass, and nitrate, potassium and sulphate availability. Nitrate availability was also positively correlated with the proportional mass of carbon lost during the decomposition experiment, suggesting that fine-root decomposition is sensitive to harvesting-induced changes in soil physicochemistry, and that variable-retention harvesting moderates the effects of harvesting on decomposition rates. These findings indicate that shortly after harvest, retention of even single trees can prevent the increase in fine-root decomposition rates associated with clearcut harvesting in these coastal Douglas-fir forests. Accordingly, management practices such as variable-retention harvesting that retain some trees in a cutblock may reduce soil C losses following forest harvesting.
机译:细根是森林土壤中的碳(c)常见的碳(c)源,而这种材料的分解可能对森林生态系统的C储存和营业额具有重要影响。森林收获改变土壤理化性质和微生物群落,这可能导致更快的分解率,但很少研究收获对细根分解的影响。可变保留收获,其中一些树木在收获后留在现场,往往导致土壤水分和温度降低,并且相对于清除收获增加了突出的异位多样性。因此,这种收获实践可能影响细根分解率。在沿海哥伦比亚的道格拉斯 - 杉木森林中,我们测得可变保留(骨料和分散装置),清除和未切割处理的细根(& 直径)分解率,并确定是否持续存在站在老年人。在可变保留处理中,我们还检查了细根分解率是否随距离固定树或保留斑块而变化。此外,我们确定了哪些土壤理化变量最能解释两年后的细根碳损失变化的变化。增加树覆盖量减缓了细根分解;在可染色体中的可变保留处理下分解的细根部缓慢分解,相对于清除处理,在这些处理中保留了15-19%的碳。细根也随着距离保留斑块的距离或保留树的距离而越来越快地分解,因为分解在聚集中心相对于开口区域中的速度较慢,在分散的保留处理中观察到类似的图案。然而,细根以森林中的类似速度分解,并具有更先进的再生,表明收获对分解率的影响并不持久。在所有采样场所,通过细根生物量和硝酸钾,硫酸钾可用来解释细根碳损失的37%的变化。硝酸盐的可用性也与分解实验中损失的比例块呈正相关,这表明细根分解对土壤物理化学的收获诱导的变化敏感,并且可变保留收获调节收获对分解率的影响。这些发现表明,收获后不久,甚至单棵树的保留可以防止与这些沿海道格拉斯冷杉森林中的清除收获相关的细根分解率的增加。因此,如可变保留收获的管理实践,以在镂空中保留一些树木可能会降低森林收获后的土壤C损失。

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